Arc-continent Collision
Arc–Continent Collision is a tectonic convergence process, belonging to the class of plate boundary interactions, wherein an intra-oceanic island arc collides with a continental margin, distinguished from other orogenic processes by the accretion of juvenile arc crust onto a passive or active continental margin following the closure of an intervening oceanic basin.
319
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22.2K
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397
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2017–2026
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Reconstructing Cenozoic SE Asia
Robert Hall · Geological Society London Special Publications · 1996 · 693 citations
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National Taiwan University
Taipei, Taiwan
18 h-index
41 publications
3.8K citations

Chinese Academy of Sciences
Beijing, China
15 h-index
60 publications
3.1K citations

Centre National de la Recherche Scientifique
Paris, France
14 h-index
37 publications
1.7K citations
National Central University
Taoyuan City, Taiwan
12 h-index
29 publications
1.4K citations
National Cheng Kung University
Tainan City, Taiwan
11 h-index
13 publications
1.3K citations
Institute of Earth Sciences, Academia Sinica
Taipei, Taiwan
10 h-index
16 publications
598 citations

China University of Geosciences (Beijing)
Beijing, China
10 h-index
28 publications
1.2K citations
Geociencias Barcelona
Barcelona, Spain
10 h-index
19 publications
856 citations
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46 publications · 3.7K citations
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